December 2017
Intermediate to advanced
392 pages
14h 52m
English
Content preview from Energy Balance Climate Models
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Chapter 3Radiation and Vertical Structure
The average vertical temperature profile of the atmosphere in steady state depends upon a balance of the divergence of the energy flux densities at each level of the atmosphere. In this chapter,1 we deal with global averages, but we retain the vertical dimension, 
. In vector notation, the divergence of a vector flux density in one (vertical) dimension is simply
3.1 
Flux density 
is a vector indicating the ...
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